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Altersbestimmung an thermalen Tiefenwässern im Oberjura des Molassebeckens mittels Krypton-Isotopen

Journal Article · · Grundwasser
 [1];  [1];  [2];  [3];  [3];  [4];  [4];  [5];  [6]
  1. Hydroisotop GmbH, Schweitenkirchen (Deutschland)
  2. Univ. of Bern, Bern (Schweiz)
  3. Argonne National Lab. (ANL), Lemont, IL (United States)
  4. Abt. 9 – Landesamt f. Geologie (Deutschland)
  5. Bayerisches Landesamt für Umwelt, Augsburg (Deutschland)
  6. Montanuniversität, Leoben (Osterreich)
81Kr (half-life 229,000 years) is an ideal tracer for old groundwater. The Upper Jurassic rock in the deep Molasse Basin is an outstanding geothermal groundwater reservoir (with temperatures up to 140 °C). However, due to the complex groundwater evolution (ion and isotope exchange, gas flux, etc.), comprehensive hydrogeological studies completed to date, including 14C–DIC and He isotopes, could not resolve the recharge dynamics and residence times. Nine geothermal wells were therefore sampled for 81Kr/85Kr employing the laser-based atom trap tracer analysis technique (ATTA). In the western and central basin, the results reveal predominant groundwater recharge during the last glacial period with one sample influenced by infiltration during the earlier glacial period. Recharge signatures and 81Kr-model-ages fit very well to subglacial recharge with cross-formational flow through the sedimentary cover (600 to >3000 m deep). In the eastern basin, the results point to the Cromerian complex, indicating a slower flow system with less influence from recharge during glacial periods.
Research Organization:
Argonne National Lab. (ANL), Argonne, IL (United States)
Sponsoring Organization:
Hydroisotop GmbH
Grant/Contract Number:
AC02-06CH11357
OSTI ID:
1580732
Alternate ID(s):
OSTI ID: 23014063
Journal Information:
Grundwasser, Journal Name: Grundwasser Journal Issue: 4 Vol. 24; ISSN 1430-483X
Country of Publication:
United States
Language:
English

References (3)


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